Spatial Variations in Crustal and Mantle Anisotropy Across the North American‐Caribbean Boundary on Haiti-Reference-Cited by-同舟云学术

Spatial Variations in Crustal and Mantle Anisotropy Across the North American‐Caribbean Boundary on Haiti

Published:2020-05-30 Issue:6 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Possee Daniel¹^ORCID,Keir Derek¹²^ORCID,Harmon Nicholas¹^ORCID,Rychert Catherine¹^ORCID,Eakin Caroline³^ORCID,Rolandone Frédérique⁴^ORCID,Leroy Sylvie⁴^ORCID,Corbeau Jordane⁵⁶^ORCID,Stuart Graham⁷,Boisson Dominique⁸,Momplaisir Roberte⁸,Prépetit Claude⁹

Affiliation:

1. School of Ocean and Earth Science, National Oceanography Centre University of Southampton Southampton UK

2. Dipartimento di Scienze della Terra Università degli Studi di Firenze Florence Italy

3. Research School of Earth Sciences The Australian National University Acton ACT Australia

4. Sorbonne Université, CNRS‐INSU, Institut des Sciences de la Terre Paris (ISTeP) Paris France

5. Université de Paris, Institut de Physique du Globe de Paris, CNRS Saint‐Pierre France

6. Observatoire Volcanologique et Sismologique de Martinique, IPGP, CNRS Saint‐Pierre France

7. School of Earth and Environment University of Leeds Leeds UK

8. Faculté des Sciences Université d'Etat d'Haïti Port‐au‐Prince Haiti

9. L'Unité Technique de Sismologie (UTS)/BME Port‐au‐Prince Haiti

Funder

Natural Environment Research Council

Australian Research Council

European Research Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB018438

Reference74 articles.

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4. Significant Earthquakes on the Enriquillo Fault System, Hispaniola, 1500-2010: Implications for Seismic Hazard

5. Character of the Caribbean–Gônave–North America plate boundaries in the upper mantle based on shear‐wave splitting

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